AVO reported that the eruption at Pavlof was ongoing during 2-8 March. Small explosions were detected on most days. Lava effusion likely continued from a vent just E of the summit, possibly sending lava flows a short distance down the NE flank, though weather clouds often obscured views. Elevated surface temperatures were often identified in satellite images. A high-resolution satellite image acquired during 5-6 March showed a developing spatter cone in the E crater, as well as no active lava flows nor widespread ash deposits on the flanks. The Volcano Alert Level remained at Watch and the Aviation Color Code remained at Orange.

Geological Summary. The most active volcano of the Aleutian arc, Pavlof is a Holocene stratovolcano that was constructed along a line of vents extending NE from the Emmons Lake caldera. Pavlof and Pavlof Sister to the NE form a dramatic pair of symmetrical, glacier-covered stratovolcanoes that overlook Pavlof and Volcano bays. Little Pavlof is a smaller cone on the SW flank of Pavlof volcano, near the rim of Emmons Lake caldera. Unlike Pavlof Sister, eruptions have frequently been reported from Pavlof, typically Strombolian to Vulcanian explosive eruptions from the summit vents and occasional lava flows. The active vents lie near the summit on the north and east sides. The largest recorded eruption took place in 1911, at the end of a 5-year-long eruptive episode, when a fissure opened on the N flank, ejecting large blocks and issuing lava flows.

Source: US Geological Survey Alaska Volcano Observatory (AVO)